“…Immediately after wave breaking, the newly created bubbles are typically of sizes 0.1 -10 mm (Deane, 1997;Haines and Johnson, 1995;Phelps et al, 1997;Zhang et al, 2002). Once bubble creation processes cease, the newly formed bubble plume evolves under the influence of turbulent diffusion, advection, buoyant degassing and dissolution, leaving behind a diffuse cloud of microbubbles (Baldy, 1988;Baldy and Bourguel, 1985;Breitz and Medwin, 1989;Cartmill and Su, 1993;Johnson and Cooke, 1979;Kolovayev, 1976;Leeuw and Cohen, 1995;Phelps and Leighton, 1998;Su and Cartmil, 1994;Su et al, 1988;Terrill et al, 2001;Farmer, 1992, 1998;Walsh and Mulhearn, 1987). Copious amounts of bubbles have also been observed in quiescent seas (Fig.…”